Results 81 to 90 of about 1,440 (281)

Petrology and geochemistry of Late Proterozoic hornblende gabbros from southeast of Fariman, Khorasan Razavi province, Iran

open access: yesJournal of Economic Geology, 2015
Introduction Hornblende-bearing gabbroic rocks are quite common in subduction-related magmatic suites and considered to represent magmatic differentiation process in arc magmas (Heliker, 1995; Hickey-Vargas et al., 1995; Mandal and Ray, 2012).
Seyed Masoud Homam
doaj  

Petrogenesis of melanite-garnets in monzodiorites from SW of Jandaq (NW of Central-East Iranian Microcontinent)

open access: yesJournal of Economic Geology
The Godar-e-Siah Eocene monzodiorite stock is located in the southwest of the Jandaq area (NE of Isfahan) and northwest of the Central-East Iranian Microcontinent (CEIM). The main minerals in these monzodiorites are plagioclase, K-feldspar, clinopyroxene,
Ahmad Jamshidzaei   +2 more
doaj   +1 more source

^DOWNLOAD E.B.O.O.K.# Principles of Igneous and Metamorphic Petrology (2nd Edition) *Full Online

open access: green, 2020
^DOWNLOAD E.B.O.O.K.# Principles of Igneous and Metamorphic Petrology (2nd Edition) *Full Online
openalex   +2 more sources

Petrología y Estructura del Complejo Ígneo-Metamórfico Aluminé, Provincia de Neuquén, Argentina Petrology and Structure of the Aluminé Igneous-Metamorphic Complex, Neuquén province, Argentina

open access: yesAndean Geology, 2011
En la presente contribución se dan a conocer los resultados parciales de un estudio de detalle de los eventos magmáticos, metamórficos y tectónicos acaecidos en el Complejo Ígneo-Metamórfico Aluminé (CIMA). Se define como CIMA al conjunto de rocas ígneas
Ivana A Urraza   +4 more
doaj  

Ultrahigh Pressure Metamorphism: Cambridge Topics in Petrology

open access: yesEos, Transactions American Geophysical Union, 1996
The field of ultra‐high pressure metamorphism (UHPM) emerged only 12 years ago when microscopic relics of coesite were found in crustal rocks that had been metamorphosed during subduction related to continental collision. Coesite‐bearing metamorphic rocks were soon found elsewhere, and then metamorphic microdiamonds were discovered.
openaire   +1 more source

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